Saturated thixotropic soil.
Saturated hydraulic conductivity is a quantitative measure of a saturated soil's ability to transmit water when subjected to a hydraulic gradient. It can be thought of as the ease with which pores of a saturated soil permit water movement.
Soil is saturated when it has reached its maximum water content; if any more is added, it will either drain downward or turn the soil into mud.
Apparently, the mass of water is simply the difference between saturated soil mass and the dried soil mass and this is 0.25 kg. - grade
Saturated soil. Shaking it results in liquefaction where the soil acts like a liquid causing massive damage to any building built on it.
Another name for saturated soil could be soil liquefaction.
Saturated thixotropic soil.
Saturated hydraulic conductivity is a quantitative measure of a saturated soil's ability to transmit water when subjected to a hydraulic gradient. It can be thought of as the ease with which pores of a saturated soil permit water movement.
Soil is saturated when it has reached its maximum water content; if any more is added, it will either drain downward or turn the soil into mud.
when the voids of soil are just filled by water the soil mass is called saturated and when soil mass is submerged in water means the water level is above the the soil level or soil mass is drowned in water then soil mass is called submerged.
It can shake it about so that it liquefies.
The soil in a region is saturated, and rainfall is greater than the need for the moisture.
mud slides
rich and saturated with water
they drown
Saturated.
If the soil is impervious clay, or the soil is already saturated by rain.